摘要
大水金矿属微细粒浸染型金矿,产于西秦岭南缘中三叠统碳酸盐岩中,矿体主要受近东西向及南北向断裂构造叠加控制。本文通过对其成矿地质特征的研究,总结分析了它的控矿因素,以期为外围找矿提供依据,为矿山生产服务。
the microgranular disseminated deposits in the south,west qinling Triassic carbonate,mainly by the ore near eastwestward tectonic superposition and south-north fracture.Based on the study of metallogenic geologic characteristics,analyses its ore-controlling factors,in order to provide basis for the periphery prospecting for mine production services.
出处
《甘肃冶金》
2011年第1期67-70,共4页
Gansu Metallurgy
关键词
金矿床
地质特征
控矿因素
大水
gold deposits
geological characteristics
ore-controlling factors
Dashui
